Toggle menu
37
137
1
720
cornish semiconductor corporation
Toggle preferences menu
Toggle personal menu
Not logged in
Your IP address will be publicly visible if you make any edits.

Perikon diode

From cornish semiconductor corporation
Revision as of 22:00, 12 September 2026 by Cornish semiconductor (talk | contribs) (→Natural Perikon diodes)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)

The Perikon detector has always been a bit of a famous and mythical beast:

At Fig. 11 we have the Perikon Detector developed by G. W. Pickard. This detector consists of two crystals--copper pyrites (Cu Fe S2) and zincite (zinc oxide ZnO), held in firm contact against each other in the manner shown. The copper pyrite crystal is mounted in a cup mounted on a spring-actuated rod provided with a suitable knob, by which it can be swung in any direction. Zincite crystals are mounted in a large cup containing several pockets, the mounting of both of the minerals being effected with a low fusing solder, Wood's metal or Hugonium alloy. The action of the Perikon detector is supposed to be based on the rectifying principle previously described; that is, it will pass current in one direction but not in the other, and thus the incoming radio frequency oscillating (alternating) currents in the aerial are rectified and caused to give a sound in the high resistance 'phones connected to the detector. This detector is invariably used with a battery of about two cells and the potential applied regulated by a potentiometer. When using a battery the polarity of the current must be such that the positive wire is connected to the copper pyrite crystal. - The Electrical Experimenter, January, 1917

Zincite is not common at all in Cornwall, although it is present at one smelting (slag) locality, presumably in tiny amounts. It is, in fact very rare in nature - occurring in some meteorites. It's much easier to get from synthetic sources, apparently it crystallises in chimneys - mostly from a zinc smelter in Silesia, Poland. I bought some online, and given that it comes from Poland, was only £4, and is very gemmy - it'll be from one of those chimneys.

This was a very basic, stupid test I didn't think would work, I checked the zincite was conductive, this always seems odd for a transparent mineral (it has a pretty high resistance). I paired it with chalcopyrite ('copper pyrites') from Ale & Cakes mine, Gwennap. The chalcopyrite is connected with the aluminum foil at the back making an normal 'ohmic' connection.

The result is actually quite amazing. This does not rely on a point contact at all, you need to press the crystals together quite hard for it to work. There is also no other form of conductivity, it's either not conducting or it's providing this really well formed curve. It's not leaky at all, it's very flat to the left of zero, only slightly showing some leakiness at the very end (-2.5V) which might well be an artifact.

I wonder how long it took Greenleaf Whittier Pickard to find this, and how many materials he went through! This is close to how the methods using silicon work today, with differently treated silicon being brought into close contact (or being modified with different patterns in the case of integrated circuits).

It does invite investigation of different minerals. I tried chalcopyrite-galena but it only really created similar results to using a cat's whisker.

Natural Perikon diodes

Sometimes two different semiconducting minerals can grow together, with their crystals butted up against each other. I'm not sure if these really count as Perikon diodes but the principal could be similar, so I'm recording it here.

One such example I've found is galena and pyrite from Ale & Cakes mine. I tested this with a otherwise normal cat's whisker and tin foil set up and had some quite strange results I don't fully understand.

These plots are the strangest I've seen. They are showing quite strong and reproducible negative resistance and need more exploration as to what is going on. I think they are 'upside down' but it's looking like the one on the right is passing current in the left side negative section until it reaches a very high level of positive conducting until about +1V when it suddenly reduces the current right down and it starts acting like an insulator. The interesting thing is that these sudden jumps are more characteristic of chalcocite than either pyrite or galena.